Organic geochemistry of an Upper Jurassic – Lower Cretaceous mudstone succession in a narrow graben setting, Wollaston Forland Basin, North-East Greenland
The Oxfordian–Ryazanian was a period of widespread deposition of marine organic-rich mudstones in basins formed during the early phases of the rifting that heralded the formation of the present-day North Atlantic. Occasionally, uninterrupted deposition prevailed for 20 million years or more. Today,...
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| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
Geological Survey of Denmark and Greenland
2023-12-01
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| Ráidu: | GEUS Bulletin |
| Fáttát: | |
| Liŋkkat: | https://geusbulletin.org/index.php/geusb/article/view/8320/14434 |
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